Zobrazeno 1 - 10
of 82
pro vyhledávání: '"Philip M. Barnes"'
Autor:
Heather M. Savage, Srisharan Shreedharan, Åke Fagereng, Julia K. Morgan, Francesca Meneghini, Maomao Wang, David D. McNamara, Laura M. Wallace, Demian M. Saffer, Philip M. Barnes, Katerina E. Petronotis, Leah J. LeVay
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 8, Pp n/a-n/a (2021)
Abstract Quantifying fault damage zones provides a window into stress distribution and rheology around faults. International Ocean Discovery Program (IODP) Expeditions 372/375 drilled an active thrust splay fault within the Hikurangi subduction margi
Externí odkaz:
https://doaj.org/article/c8da92d3ec1a4728b7b4ef24d6f257c8
Autor:
Hannu Seebeck, Russ Van Dissen, Nicola Litchfield, Philip M. Barnes, Andrew Nicol, Robert Langridge, David J. A. Barrell, Pilar Villamor, Susan Ellis, Mark Rattenbury, Stephen Bannister, Matthew Gerstenberger, Francesca Ghisetti, Rupert Sutherland, Hamish Hirschberg, Jeff Fraser, Scott D. Nodder, Mark Stirling, Jade Humphrey, Kyle J. Bland, Andrew Howell, Joshu Mountjoy, Vicki Moon, Timothy Stahl, Francesca Spinardi, Dougal Townsend, Kate Clark, Ian Hamling, Simon Cox, Willem de Lange, Paul Wopereis, Mike Johnston, Regine Morgenstern, Genevieve Coffey, Jennifer D. Eccles, Timothy Little, Bill Fry, Jonathan Griffin, John Townend, Nick Mortimer, Samantha Alcaraz, Cécile Massiot, Julie V. Rowland, James Muirhead, Phaedra Upton, Julie Lee
Publikováno v:
New Zealand Journal of Geology and Geophysics. :1-21
Autor:
Adam Woodhouse, Philip M. Barnes, Anthony Shorrock, Lorna J. Strachan, Martin Crundwell, Helen C. Bostock, Jenni Hopkins, Steffen Kutterolf, Katharina Pank, Erik Behrens, Annika Greve, Rebecca Bell, Ann Cook, Katerina Petronotis, Leah LeVay, Robert A. Jamieson, Tracy Aze, Laura Wallace, Demian Saffer, Ingo Pecher
Glacio-eustatic cycles lead to changes in sedimentation on all types of continental margins. There is, however, a paucity of sedimentation rate data over eustatic sea-level cycles in active subduction zones. During International Ocean Discovery Progr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f5316a5d357daf8ec634f7a715560d70
https://doi.org/10.1080/00288306.2022.2099432
https://doi.org/10.1080/00288306.2022.2099432
Autor:
Yoshihiro Kaneko, Jamie Howarth, Scott D. Nodder, M. Namık Çağatay, Philip M. Barnes, Helen C Bostock, Alan R. Orpin, Caroline Holden, Lorna J. Strachan, Katie Jones, Joshu J. Mountjoy
Publikováno v:
Nature Geoscience. 14:161-167
Turbidite palaeoseismology has produced arguably the most comprehensive multimillennial scale records of subduction-zone earthquakes but is underpinned by techniques that are vigorously debated in earthquake science. Resolving this argument requires
Autor:
Maomao Wang, Philip M. Barnes, Julia K. Morgan, Rebecca E. Bell, Gregory F. Moore, Ming Wang, Ake Fagereng, Heather Savage, Davide Gamboa, Robert N. Harris, Stuart Henrys, Joshu Mountjoy, Anne M. Tréhu, Demian Saffer, Laura Wallace, Katerina Petronotis
Publikováno v:
Earth and Planetary Science Letters. 605:118022
Calcareous rocks are commonly found in subduction zones, but few studies have investigated the consolidation and compactive deformation of these rocks prior to subduction, and their potential effects on subduction and accretionary processes are thus
Autor:
Stuart Henrys, Sam R. Davidson, Jarg R. Pettinga, Andrew Nicol, Joshu J. Mountjoy, Philip M. Barnes
Publikováno v:
Geology. 48:493-498
The initial stages of seamount subduction and associated deformation in an overriding accretionary wedge is rarely documented. Initial subduction of Bennett Knoll seamount and faulting of the overlying strata along the Hikurangi subduction margin, Ne
Highlights • Gas hydrate systems modelling reproduces concentrated gas hydrates indicated by high amplitude seismic reflections. • Spatially variable rates in microbial gas generation beneath the hydrate stability zone drive gas hydrate formation
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a1f9f29a6744606e039f6b49f575ef2e
https://doi.org/10.1016/j.marpetgeo.2021.105394
https://doi.org/10.1016/j.marpetgeo.2021.105394
Autor:
Julia K. Morgan, Evan A. Solomon, Ake Fagereng, Heather M. Savage, Maomao Wang, Francesca Meneghini, Philip M. Barnes, Rebecca E. Bell, Melodie E. French, Nathan L. Bangs, Hiroko Kitajima, Demian M. Saffer, Laura M. Wallace
Publikováno v:
Earth and Planetary Science Letters. 593:117651
IODP Site U1518, drilled during IODP Expeditions 372 and 375, penetrated a large-offset (∼6 km) thrust, the Pāpaku fault, rising from a megathrust that hosts recurring slow slip events along the Hikurangi margin. Although drilling intersected the
Autor:
Carolyn Boulton, Susanne Buiter, Francesca Ghisetti, Philip M. Barnes, Ake Fagereng, Susan Ellis
Publikováno v:
Geophysical Journal International
SUMMARYThe southcentral Hikurangi subduction margin (North Island, New Zealand) has a wide, low-taper accretionary wedge that is frontally accreting a >3-km-thick layer of sediments, with deformation currently focused near the toe of the wedge. We us
Autor:
Demian M. Saffer, Maomao Wang, Katerina Petronotis, Srisharan Shreedharan, Julia K. Morgan, Leah J. LeVay, Francesca Meneghini, David D. McNamara, Heather M. Savage, Laura M. Wallace, Philip M. Barnes, Ake Fagereng
Publikováno v:
Geochemistry, Geophysics, Geosystems
Quantifying fault damage zones provides a window into stress distribution and rheology around faults. International Ocean Discovery Program (IODP) Expeditions 372/375 drilled an active thrust splay fault within the Hikurangi subduction margin. The fa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::48a713b581b3039cc3000db89a0e802c
http://hdl.handle.net/11568/1115838
http://hdl.handle.net/11568/1115838